DOCSLIB.ORG

Sedimentary Geology of the Middle Carboniferous of the Donbas Region

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Sedimentary Geology of the Middle Carboniferous of the Donbas Region OPEN Sedimentary geology of the middle SUBJECT AREAS: Carboniferous of the Donbas region GEOLOGY SEDIMENTOLOGY (Dniepr-Donets basin, Ukraine) Douwe J. J. van Hinsbergen1, Hemmo A. Abels1, Wolter Bosch1, Flora Boekhout2, Alexander Kitchka4, Received Maartje Hamers1, Douwe G. van der Meer3, Mark Geluk5 & Randell A. Stephenson6 8 September 2014 Accepted 1Department of Earth Sciences, University of Utrecht, Budapestlaan 4, 3584 CD Utrecht, the Netherlands, 2Institut fu¨r Geologie und 28 January 2015 Pala¨ontologie, Westfa¨lische Wilhelms-Universita¨t, Corrensstrasse 24, 48149 Mu¨nster, 3Nexen Petroleum UK Ltd., Charter Place, Vine Street, Uxbridge, Middlesex, UB8 1JG, United Kingdom, 4SE NaukaNaftogaz Res. Inst., NJSC Naftogaz of Ukraine, 8 Kyivska Published St., 08132 Vyshneve, Ukraine, 5Shell International Exploration and Production B.V., Kessler Park 1, 2288 GS Rijswijk, the 20 March 2015 Netherlands, 6School of Geosciences, Meston Building, King’s College, University of Aberdeen, Aberdeen AB24 3UE, UK. Correspondence and The Paleozoic Dniepr-Donets Basin in Belarus, Ukraine, and Russia forms a major hydrocarbon province. Although well- and seismic data have established a 20 km thick stratigraphy, field-studies of its sediments requests for materials are scarce. The inverted Donbas segment (Ukraine) exposes the middle Carboniferous part of the basin’s should be addressed to stratigraphy. Here, we provide detailed sedimentological data from 13 sections that cover 1.5 of the total of D.J.J.H. (d.j.j. 5 km of the Bashkirian and Moscovian stages and assess the paleoenvironment and paleo-current [email protected]) directions. Middle Carboniferous deposition occurred in a shelf environment, with coal deposition, subordinate fluvial facies, and abundant lower and middle shoreface facies, comprising an intercalated package of potential source and reservoir rocks. Sedimentary facies indicate a paleodepth range from below storm wave base to near-coastal swamp environments. Sedimentation and subsidence were hence in pace, with subtle facies changes likely representing relative sea-level changes. Paleocurrent directions are remarkably consistently southeastward in time and space in the different sedimentary facies across the Donbas Fold Belt, illustrating a dominant sedimentary infill along the basin axis, with little basin margin influence. This suggests that the middle Carboniferous stratigraphy of the Dniepr-Donets basin to the northwest probably contains significant amounts of fluvial sandstones, important for assessing hydrocarbon reservoir potential. he Dniepr-Donets Basin (DDB) forms a major hydrocarbon and coal basin in Eastern Europe with signifi- cant commercial significance1–7, forming a intra-cratonic, deep rift with up to 22 km of sediment1,8 that T underwent its main basin fill history between the late Devonian and Permian9–11. It is located between the Ukrainian Shield to the south and the Voronezh Massif to the north, in the southwest of the East European Craton (EEC; Fig. 1). The basin’s infill is poorly exposed, and knowledge about its sedimentary evolution largely relies on subsurface data. The eastern part of the basin, however, has been inverted in Permian and younger times and forms the Donbas Foldbelt, where Devonian and younger (volcano-) sedimentary rocks of the DDB are exposed12,13. The Donbas Foldbelt is characterised by WNW-ESE trending long-wavelength folds and faults14,15 (Fig. 1). As a result of Permian and/or Late Cretaceous/Paleogene inversion of the Donbas Foldbelt16–19, Carboniferous sedi- ments are exposed. The middle Carboniferous is exposed within the axial zone of the Donbas Foldbelt as well as near the southern margin, where it overlies pre-and syn-rift Devonian to Lower Carboniferous sediments. Outcrops in the Donbas Foldbelt are mainly confined to road and river sections and quarries. We present detailed sedimentological descriptions and paleoenvironmental interpretations from 13 sections covering 1.5 km of a total of ,5 km Bashkirian and Moscovian stratigraphy. We briefly discuss the potential implications of our findings for the sedimentary geology of the DDB farther to the northwest, where exposures of the middle Carboniferous are absent. Geological setting. The DDB overlies an Archean to Lower Proterozoic crystalline basement20,21 and trends NW- SE from Belarus through Ukraine to Russia, connecting with the Karpinsky Swell to the east (Fig. 1). The Donbas segment of the DDB formed at the southern margin of the EEC, which belonged to Laurussia in the Late Paleozoic SCIENTIFIC REPORTS | 5 : 9099 | DOI: 10.1038/srep09099 1 www.nature.com/scientificreports Figure 1 | Geological map of the Donbas Foldbelt, and in the inset, the location of the Donbas in the regional East European structural framework (modified from Stovba and Stephenson31). and was located at near-equatorial latitudes during the Early Carbo- A post-rift sag sequence is bounded by pre-Carboniferous and niferous moving to ,15u northerly latitudes in the Permian22–25. pre-Triassic unconformities12. Following the first stages of rift react- Towards the southeast, the width and thickness of the basin fill, the ivation in the Visean, the Ukrainian shield was covered by a thin layer intensity of inversion-related deformation, the degree of metamorphism of upper Visean and younger sediments. A large volume of fluvial of its exposed sediments, as well as the degree of syn-rift volcanic clastic material was transported by river systems from the northwest activity increase26. Basin inversion occurred in two or three phases in along the basin axis, prograding into a deeper water basin that existed Permo-Triassic and Late Cretaceous-Early Cenozoic time16–19. since Devonian time39. Serpukhovian and younger Carboniferous Shortening of the Donbas Foldbelt may be Permian27–30 or Late sediments commonly consist of cyclothems of marine limestone or Cretaceous-Early Cenozoic in age31,32. Inversion occurred along shale at the bottom to coal and paleosol beds at the top and form the WNW-ESE rift-bounding faults, and formed a central ‘Main focus of this study40. Anticline’33 flanked by gentle folds. To the north, the Donbas Foldbelt During the Carboniferous and much of the Early Permian, the borders the Voronezh Massif (Fig. 1) along large thrusts and reverse DDB gradually subsided. The rate of subsidence was high; the thick- faults; in the south the contact of the Donbas Foldbelt with the ness of the Carboniferous-Lower Permian, dominantly clastic stra- Ukrainian Shield is formed by reverse faults8,32. tigraphy increases from 2–3 km in the northwest to about 11 km in Sedimentation in the DDB started in Middle Devonian time with the southeast of the basin. Increased aridity and relative sea level fall deposition of pre-rift sediments under platform conditions. Judging during the early Permian resulted in deposition of red beds, carbo- from the absence of marginal facies, and based on low-temperature nates, and evaporites16,41–44. Upper Permian sedimentary rocks are geochronology, that platform originally extended far beyond the absent and post-Permian deposits are fluvio-lacustrine to shallow present limits of the basin34,35. The main rifting phase that formed marine clastics and carbonates with a maximum thickness of ,2– the DDB started in the Late Devonian (370–363 Ma36,37 and was 2.5 km12. associated with basement doming and mafic to intermediate mag- The Carboniferous stratigraphy of the Donbas region studied here matism13. Devonian rifting led to widespread salt-deposition, has been divided into lithostratigraphical suites45. Four suites are reflected by local diapirs in the Donbas Foldbelt38. Salt formations recognized in the Mississippian, nine in the Early and Middle probably filled deep-water basins, and were preceded by deposition Pennsylvanian (or Bashkirian and Moscovian; Fig. 2). The ‘middle’ of organic-rich anoxic shales and carbonates2. Uppermost Devonian Carboniferous is more than 5 km thick (,3 km Bashkirian and 2– rocks formed large sub-aqueous clastic fans along the southern basin 2.5 km of Moscovian12,46,47). Limestone beds form regional markers margin and containing shales interbedded in coarser clastics. A total in the successive suites and have been labelled with a letter from the thickness of 4–5 km of the syn-rift basin infill was estimated2. Latin alphabet accordingly. Smaller or regionally less coherent lime- SCIENTIFIC REPORTS | 5 : 9099 | DOI: 10.1038/srep09099 2 www.nature.com/scientificreports stone beds within suites were assigned subscript successive numbers (Fig. 2). Additional subdivision has been made on the basis of the fossil content of the succession. Biozones have been coded differently from the suites, and the boundaries do not all correspond with the suite boundaries (Fig. 2). Biostratigraphy and suites subdivision form the basis for correlation of the Donbas stratigraphy to the Western European and American stratigraphies48. Results Thirteen sections in the Donbas region were studied in detail (Figs. 1, 2, 3), covering over 1.5 of the total of ,5 km of middle Carboniferous stratigraphy (Fig. 2). The studied sections together represent the majority of available outcrops of Bashkirian and Moscovian stra- tigraphy in the area. Extensive descriptions of each section are given in the Supplementary Material, with detailed sedimentary logs, descriptions, field photographs and section locations. Here, we briefly describe the sections in stratigraphic order. The oldest part of the stratigraphy was studied in the
Load more

Recommended publications
  • Assembly, Configuration, and Break-Up History of Rodinia
    Author's personal copy Available online at www.sciencedirect.com Precambrian Research 160 (2008) 179–210 Assembly, configuration, and break-up history of Rodinia: A synthesis Z.X. Li a,g,∗, S.V. Bogdanova b, A.S. Collins c, A. Davidson d, B. De Waele a, R.E. Ernst e,f, I.C.W. Fitzsimons g, R.A. Fuck h, D.P. Gladkochub i, J. Jacobs j, K.E. Karlstrom k, S. Lu l, L.M. Natapov m, V. Pease n, S.A. Pisarevsky a, K. Thrane o, V. Vernikovsky p a Tectonics Special Research Centre, School of Earth and Geographical Sciences, The University of Western Australia, Crawley, WA 6009, Australia b Department of Geology, Lund University, Solvegatan 12, 223 62 Lund, Sweden c Continental Evolution Research Group, School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia d Geological Survey of Canada (retired), 601 Booth Street, Ottawa, Canada K1A 0E8 e Ernst Geosciences, 43 Margrave Avenue, Ottawa, Canada K1T 3Y2 f Department of Earth Sciences, Carleton U., Ottawa, Canada K1S 5B6 g Tectonics Special Research Centre, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia h Universidade de Bras´ılia, 70910-000 Bras´ılia, Brazil i Institute of the Earth’s Crust SB RAS, Lermontova Street, 128, 664033 Irkutsk, Russia j Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway k Department of Earth and Planetary Sciences, Northrop Hall University of New Mexico, Albuquerque, NM 87131, USA l Tianjin Institute of Geology and Mineral Resources, CGS, No.
    [Show full text]
  • Ages of Detrital Zircons (U/Pb, LA-ICP-MS) from the Latest
    Precambrian Research 244 (2014) 288–305 Contents lists available at ScienceDirect Precambrian Research jo urnal homepage: www.elsevier.com/locate/precamres Ages of detrital zircons (U/Pb, LA-ICP-MS) from the Latest Neoproterozoic–Middle Cambrian(?) Asha Group and Early Devonian Takaty Formation, the Southwestern Urals: A test of an Australia-Baltica connection within Rodinia a,∗ b c Nikolay B. Kuznetsov , Joseph G. Meert , Tatiana V. Romanyuk a Geological Institute, Russian Academy of Sciences, Pyzhevsky Lane, 7, Moscow 119017, Russia b Department of Geological Sciences, University of Florida, 355 Williamson Hall, Gainesville, FL 32611, USA c Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, B. Gruzinskaya ul. 10, Moscow 123810, Russia a r t i c l e i n f o a b s t r a c t Article history: A study of U-Pb ages on detrital zircons derived from sedimentary sequences in the western flank of Received 5 February 2013 Urals (para-autochthonous or autochthonous with Baltica) was undertaken in order to ascertain/test Received in revised form source models and paleogeography of the region in the Neoproterozoic. Samples were collected from the 16 September 2013 Ediacaran-Cambrian(?) age Asha Group (Basu and Kukkarauk Formations) and the Early Devonian-aged Accepted 18 September 2013 Takaty Formation. Available online 19 October 2013 Ages of detrital zircons within the Basu Formation fall within the interval 2900–700 Ma; from the Kukkarauk Formation from 3200 to 620 Ma. Ages of detrital zircons from the Devonian age Takaty For- Keywords: Australia mation are confined to the Paleoproterozoic and Archean (3050–1850 Ma).
    [Show full text]
  • A Seismic Model for Moho and Crustal Structure in Europe, Greenland, and the North Atlantic Region☆
    Tectonophysics 609 (2013) 97–153 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region☆ Irina M. Artemieva ⁎, Hans Thybo IGN, University of Copenhagen, Denmark article info abstract Article history: We present a new digital crustal model for Moho depth and crustal structure in Europe, Greenland, Iceland, Received 27 November 2012 Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W–62E, 30N–84N). Our compilation is based Received in revised form 18 July 2013 on digitization of original seismic profiles and Receiver Functions from ca. 650 publications which provides a Accepted 4 August 2013 dense regional data coverage. Exclusion of non-seismic data allows application of the database to potential Available online 15 August 2013 field modeling. EUNAseis model includes Vp velocity and thickness of five crustal layers, including the sedimen- tary cover, and Pn velocity. For each parameter we discuss uncertainties associated with theoretical limitations, Keywords: Moho regional data quality, and interpolation. Crustal thickness By analyzing regional trends in crustal structure and links to tectonic evolution illustrated by a new tectonic map, Crystalline crust we conclude that: (1) Each tectonic setting shows significant variation in depth to Moho and crustal structure, Sedimentary cover essentially controlled by the age of latest tectono-thermal processes; (2) Published global averages of crustal pa- Pn velocity rameters are outside of observed ranges for any tectonic setting in Europe; (3) Variation of Vp with depth in the Crustal evolution sedimentary cover does not follow commonly accepted trends; (4) The thickness ratio between upper-middle (Vp b 6.8 km/s) and lower (Vp N 6.8 km/s) crystalline crust is indicative of crustal origin: oceanic, transitional, platform, or extended crust; (5) Continental rifting generally thins the upper-middle crust significantly without changing Vp.
    [Show full text]
  • Central Pontides, Northern Turkey ⇑ Remziye Akdog˘An A,B,D, , Aral I
    Journal of Asian Earth Sciences 134 (2017) 309–329 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Full length Article Provenance of a large Lower Cretaceous turbidite submarine fan complex on the active Laurasian margin: Central Pontides, northern Turkey ⇑ Remziye Akdog˘an a,b,d, , Aral I. Okay a,b, Gürsel Sunal a, Gabor Tari c, Guido Meinhold d, Andrew R.C. Kylander-Clark e a Istanbul Technical University, Faculty of Mines, Department of Geology, Maslak 34469, Turkey b Istanbul Technical University, Eurasia Institute of Earth Sciences, Maslak 34469, Turkey c OMV Exploration and Production, Trabrennstrabe 6-8, Vienna 1020, Austria d Geowissenschaftliches Zentrum der Universität Göttingen, Abteilung Sedimentologie/Umweltgeologie, Goldschmidtstrabe 3, D-37077 Göttingen, Germany e University of California Santa Barbara, Department of Earth Sciences, Santa Barbara, CA 93106, USA article info abstract Article history: The Pontides formed the southern active margin of Laurasia during the Mesozoic. They became separated Received 15 April 2016 from mainland Laurasia during the Late Cretaceous, with the opening of the Black Sea as an oceanic back- Received in revised form 19 November 2016 arc basin. During the Early Cretaceous, a large submarine turbidite fan complex developed in the Central Accepted 24 November 2016 Pontides. The turbidites cover an area of 400 km by 90 km with a thickness of more than 2 km. We have Available online 25 November 2016 investigated the provenance of these turbidites—the Çag˘layan Formation—using paleocurrent measure- ments, U-Pb detrital zircon ages, REE abundances of dated zircons and geochemistry of detrital rutile Keywords: grains.
    [Show full text]
  • Late Precambrian to Triassic History of the East
    VU Research Portal Late Precambrian to Triassic history of the East European craton: dynamics of sedimentary basin evolution Nikishin, A.M.; Ziegler, P.A.; Stephenson, R.A.; Cloetingh, S.A.P.L.; Furne, A.V.; Fokin, P.A.; Ershov, A.V.; Boloytov, S.N.; Korotaev, M.V.; Alekseev, A.S.; Gorbachev, V.I.; Shipilov, E.V.; Lankreijer, A.C.; Bembinova, E.Y.; Shalimov, I.V. published in Default journal 1996 DOI (link to publisher) 10.1016/S0040-1951(96)00228-4 document version Publisher's PDF, also known as Version of record Link to publication in VU Research Portal citation for published version (APA) Nikishin, A. M., Ziegler, P. A., Stephenson, R. A., Cloetingh, S. A. P. L., Furne, A. V., Fokin, P. A., Ershov, A. V., Boloytov, S. N., Korotaev, M. V., Alekseev, A. S., Gorbachev, V. I., Shipilov, E. V., Lankreijer, A. C., Bembinova, E. Y., & Shalimov, I. V. (1996). Late Precambrian to Triassic history of the East European craton: dynamics of sedimentary basin evolution. Default journal. https://doi.org/10.1016/S0040-1951(96)00228-4 General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim.
    [Show full text]
  • Palynology of Jurassic (Bathonian) Sediments from Donbas, Northeast Ukraine
    Palaeobio Palaeoenv https://doi.org/10.1007/s12549-017-0310-3 ORIGINAL PAPER Palynology of Jurassic (Bathonian) sediments from Donbas, northeast Ukraine Olena Shevchuk1 & Sam M. Slater2 & Vivi Vajda 2 Received: 11 July 2017 /Revised: 14 September 2017 /Accepted: 26 October 2017 # The Author(s) 2018. This article is an open access publication Abstract A palynological and sedimentological study of an abundances of Gleicheniidites and higher percentages of outcrop succession adjacent to the village of Kamyanka with- Pinuspollenites and Araucariacites compared to assemblage in the Kharkiv region of northeast Ukraine was carried out. A. Another difference between the two units is the high rela- The successions occur within the Dnieper–Donets Basin, tive abundance of seed fern pollen (Alisporites) in the upper which hosts vast successions (> 20 km) of post mid- part of assemblage B. The thermal alteration index (TAI) of Devonian strata and is one of the main hydrocarbon- the palynomorphs is estimated to range from 3 to 3.5, indicat- producing basins in Europe. Middle Jurassic sandstones, silt- ing a burial depth corresponding to the mature main phase of stones and claystones represent the sedimentary successions at liquid petroleum and, to some extent, gas generation. the Kamyanska locality. Few palynological studies have been Comparisons between the miospore and macrofloral assem- performed on the Jurassic of Ukraine and even fewer present- blages show that the palynoflora and macroflora are strongly ed in the international literature. Thirty spore taxa and 21 similar at broad taxonomic levels. Importantly, the miospore pollen taxa were identified, together with taxa kept in open assemblages described here compare well with European nomenclature (e.g.
    [Show full text]
  • Mesoproterozoic Paleogeography: Supercontinent and Beyond
    NOTICE: This is the author’s version of a work that was accepted for publication in Precambrian Research. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Precambrian Research, Vol. 244, (2013). doi: 10.1016/j.precamres.2013.05.014 1 Mesoproterozoic paleogeography: supercontinent and beyond 2 Sergei A. Pisarevskya,b, Sten-Åke Elmingc, Lauri J. Pesonend, Zheng-Xiang Lia 3 a Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) 4 and the Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtain University, GPO 5 Box U1987, Perth, WA 6845, Australia. 6 bSchool of Earth and Environment, University of Western Australia, 35 Stirling Highway, 7 Crawley, WA 6009, Australia 8 cDepartment of Civil, Environmental and Natural resources engineering, Luleå University of Technology, SE- 9 07187 Luleå, Sweden. 10 dDivision of Geophysics and Astronomy, Department of Physics, University of Helsinki, PO Box 64 (Gustaf 11 Hällströmin katu 2), FIN-00014 Helsinki, Finland. 12 13 Abstract 14 A set of global paleogeographic reconstructions for the 1770–1270 Ma time interval is 15 presented here through a compilation of reliable paleomagnetic data (at the 2009 Nordic 16 Paleomagnetic Workshop in Luleå, Sweden) and geological constraints. Although currently 17 available paleomagnetic results do not rule out the possibility of the formation of a 18 supercontinent as early as ca. 1750 Ma, our synthesis suggests that the supercontinent 19 Nuna/Columbia was assembled by at least ca.
    [Show full text]
  • Re-Assessing the European Lithium Resource Potential
    Re-assessing the European lithium resource potential – A review of hard-rock resources and metallogeny Blandine Gourcerol, Eric Gloaguen, Jérémie Melleton, Johann Tuduri, Xavier Galiègue To cite this version: Blandine Gourcerol, Eric Gloaguen, Jérémie Melleton, Johann Tuduri, Xavier Galiègue. Re-assessing the European lithium resource potential – A review of hard-rock resources and metallogeny. Ore Geology Reviews, Elsevier, 2019, 109, pp.494-519. 10.1016/j.oregeorev.2019.04.015. insu-02115174 HAL Id: insu-02115174 https://hal-insu.archives-ouvertes.fr/insu-02115174 Submitted on 30 Apr 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Re-assessing the European lithium resource potential – A review of hard-rock resources and metallogeny B. Gourcerol, E. Gloaguen, J. Melleton, J. Tuduri, Xavier Galiegue PII: S0169-1368(18)30801-1 DOI: https://doi.org/10.1016/j.oregeorev.2019.04.015 Reference: OREGEO 2903 To appear in: Ore Geology Reviews Received Date: 20 September 2018 Revised Date: 15 April 2019 Accepted Date: 23 April 2019 Please cite this article as: B. Gourcerol, E. Gloaguen, J. Melleton, J. Tuduri, X. Galiegue, Re-assessing the European lithium resource potential – A review of hard-rock resources and metallogeny, Ore Geology Reviews (2019), doi: https://doi.org/10.1016/j.oregeorev.2019.04.015 This is a PDF file of an unedited manuscript that has been accepted for publication.
    [Show full text]
  • New U–Pb Ages for Mafic Dykes in the Northwestern Region of the Ukrainian Shield: Coeval Tholeiitic and Jotunitic Magmatism
    GFF ISSN: 1103-5897 (Print) 2000-0863 (Online) Journal homepage: http://www.tandfonline.com/loi/sgff20 New U–Pb ages for mafic dykes in the Northwestern region of the Ukrainian shield: coeval tholeiitic and jotunitic magmatism Leonid Shumlyanskyy, Richard E. Ernst, Ulf Söderlund, Kjell Billström, Oleksandr Mitrokhin & Stepan Tsymbal To cite this article: Leonid Shumlyanskyy, Richard E. Ernst, Ulf Söderlund, Kjell Billström, Oleksandr Mitrokhin & Stepan Tsymbal (2016) New U–Pb ages for mafic dykes in the Northwestern region of the Ukrainian shield: coeval tholeiitic and jotunitic magmatism, GFF, 138:1, 79-85, DOI: 10.1080/11035897.2015.1116602 To link to this article: http://dx.doi.org/10.1080/11035897.2015.1116602 Published online: 10 Feb 2016. Submit your article to this journal Article views: 9 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=sgff20 Download by: [Naturhistoriska Riksmuseum] Date: 01 April 2016, At: 05:04 GFF, 2016 Vol. 138, No. 1, 79–85, http://dx.doi.org/10.1080/11035897.2015.1116602 Article New U–Pb ages for mafic dykes in the Northwestern region of the Ukrainian shield: coeval tholeiitic and jotunitic magmatism LEONID SHUMLYANSKYY1, RICHARD E. ERNST2, ULF SÖDERLUND3,4, KJELL BILLSTRÖM4, OLEKSANDR MITROKHIN5 and STEPAN TSYMBAL1 Shumlyanskyy, L., Ernst, R. E., Söderlund, U., Billström, K., Mitrokhin, O. & Tsymbal, S., 2016: New U-Pb ages for mafic dykes in the Northwestern region of the Ukrainian shield: coeval tholeiitic and jotunitic magmatism. GFF, Vol. 138, No. 1, pp. 79–85. © Geologiska Föreningen. doi: http://dx.doi.org/10.1080/11035897.
    [Show full text]
  • Structure and Density of Sedimentary Basins in the Southern Part of the East-European Platform and Surrounding Area
    applied sciences Article Structure and Density of Sedimentary Basins in the Southern Part of the East-European Platform and Surrounding Area Mikhail K. Kaban 1,2,3, Alexei Gvishiani 2,3, Roman Sidorov 2,* , Alexei Oshchenko 2 and Roman I. Krasnoperov 2 1 German Research Center for Geosciences (GFZ), 14473 Potsdam, Germany; [email protected] 2 Geophysical Center of the Russian Academy of Sciences (GC RAS), 119296 Moscow, Russia; [email protected] (A.G.); [email protected] (A.O.); [email protected] (R.I.K.) 3 Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences (IPE RAS), 119296 Moscow, Russia * Correspondence: [email protected]; Tel.: +7-495-930-0546 Abstract: Modern satellite gravity missions and ground gravimetry provide operational data models that can be used in various studies in geology, tectonics, and climatology, etc. In the present study, sedimentary basins in the southern part of the East European Platform and adjoining areas including the Caucasus are studied by employing the approach based on decompensative gravity anomalies. The new model of sediments, implying their thickness and density, demonstrates several important features of the sedimentary cover, which were not or differently imaged by previous studies. We found a significant redistribution of the low-dense sediments in the Black Sea. Another principal feature is the increased thickness of relatively low-dense sediments in the Eastern Greater Caucasus. The deepest part of the South Caspian basin is shifted to the north, close to the Apsheron Trough. In its present position, it is almost joined with the Terek–Caspian depression, which depth is also increased.
    [Show full text]
  • How Is the European Lithosphere Imaged by Magnetotellurics?
    Surv Geophys (2007) 28:239–272 DOI 10.1007/s10712-007-9024-9 REVIEW PAPER How is the European Lithosphere Imaged by Magnetotellurics? Toivo Korja Received: 15 February 2007 / Accepted: 25 June 2007 / Published online: 21 August 2007 Ó Springer Science+Business Media B.V. 2007 Abstract I review recent investigations on the electrical conductivity of the lithosphere and asthenosphere in Europe. The principal method in the reviewed studies is the mag- netotelluric method, but in many cases other electromagnetic methods (e.g., magnetovariational profilings and geomagnetic depth soundings) have provided additional information on sub- surface conductivity or have been the primary method. The review shows that the magnetotelluric method has been used, and is being used, in all kinds of environments and for many different processes shaping the crust and lithosphere. The crust is very heterogeneous, both with respect to the scale of conductive/resistive features and interpretations: research targets vary from Archaean palaeostructures to ongoing processes. The European database of the depth to the lithosphere-asthenosphere boundary (LAB) in Europe is updated, and a new map showing lateral variations of the depth of LAB is provided. The compilation shows that (1) the Phanerozoic European lithosphere, with considerable variations (45–150 km), is much thinner than the Precambrian European lithosphere, (2) the Trans-European Suture Zone is a major electrical border in Europe separating electrically (as well as geophysically and geo- logically in general) two quite different settings, (3) the thinnest lithosphere is found under the extensional Pannonian Basin (45–90 km), (4) in most of the East European Craton there are no indications of a high conductivity zone in upper mantle.
    [Show full text]
  • Late Precambrian to Triassic History of the East European Craton: Dynamics of Sedimentary Basin Evolution
    TECTONOPHYSICS ELSEVIER Tectonophysics 268 (1996) 23-63 Late Precambrian to Triassic history of the East European Craton: dynamics of sedimentary basin evolution A.M. Nlkishin• " " a*, , P.A. Ziegler b, R.A. Stephenson c, S.A.P.L. Cloetingh c, A.V. Fume a, P.A. Fokin a, A.V. Ershov a, S.N. Bolotov a, M.V. Korotaev ", A.S. Alekseev a, V.I. Gorbachev d, E.V. Shipilov e, A. Lankreijer c, E.Yu. Bembinova a, I.V. Shalimov a a Geological Faculty, Moscow State University, Leninskie Gory, 119899 Moscow, Russia b Geological-Palaeontological Institute, University of Basel, Bernoullistr. 32, 4056 Basel, Switzerland c Vrije Universiteit, Faculty of Earth Sciences, De Boelelaan 1085, 1081 HVAmsterdam, Netherlands d NEDRA, Yaroslavl, Russia e Institute of Marine Geophysics, Murmansk, Russia Received 5 September 1995; accepted 31 May 1996 Abstract During its Riphean to Palaeozoic evolution, the East European Craton was affected by rift phases during Early, Middle and Late Riphean, early Vendian, early Palaeozoic, Early Devonian and Middle-Late Devonian times and again at the transition from the Carboniferous to the Permian and the Permian to the Triassic. These main rifting cycles were separated by phases of intraplate compressional tectonics at the transition from the Early to the Middle Riphean, the Middle to the Late Riphean, the Late Riphean to the Vendian, during the mid-Early Cambrian, at the transition from the Cambrian to the Ordovician, the Silurian to the Early Devonian, the Early to the Middle Devonian, the Carboniferous to Permian and the Triassic to the Jurassic. Main rift cycles axe dynamically related to the separation of continental terranes from the margins of the East European Craton and the opening of Atlantic-type palaeo-oceans and/or back-arc basins.
    [Show full text]